Geoscience Reference
In-Depth Information
P
Figure 5.2.
A strip of a
thin, spherical shell with
centre O. P is an arbitrary
point at distance
r
from O.
D
Q
bd
q
b
b
t
q
d
q
O
The potential of the entire spherical shell can now be evaluated from Eq. (5.6)
by integrating the potential of the strip:
=−
G
ρ
t
2
π
b
2
sin
θ
d
θ
V
(5.8)
(
r
2
+
b
2
−
2
br
cos
θ
)
1
/
2
To evaluate this integral, we need to change it from an integral over
θ
to an integral
over
D
. Differentiation of Eq. (5.7)gives
D
d
D
=
br
sin
θ
d
θ
(5.9)
Equation (5.8)isthen written
=−
G
ρ
t
2
π
b
2
D
max
d
D
br
V
(5.10)
D
min
To evaluate this integral, it is necessary to consider two situations: (i) when P is
outside the spherical shell (
r
>
b
) and (ii) when P is inside the spherical shell
(
r
b
).
(i) When the point P is
external
to the spherical shell, as in Fig. 5.2, the limits
D
min
and
D
max
are
r-b
and
r
<
+
b
, respectively, and the potential at point P is
=−
G
ρ
t
2
π
b
2
D
br
r
+
b
V
r
−
b
G
ρ
t
4
π
b
2
r
=−
(5.11)
b
2
t
, and so, at the point P the
potential of the shell is the same as that due to an equal mass placed at O, the
centre of the shell. The gravitational acceleration
a
due to the spherical shell can
be calculated from Eq. (5.4) (in spherical polar coordinates) as
a
=−
∂
V
The total mass of the spherical shell is 4
π
ρ
G
ρ
t
4
π
b
2
r
2
∂
r
=−
(5.12)